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首页> 外文期刊>Archives of Agronomy and Soil Science >Fertilization effects on organic matter of arable soils in diverse environmental conditions of the Czech Republic
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Fertilization effects on organic matter of arable soils in diverse environmental conditions of the Czech Republic

机译:捷克共和国各种环境条件下耕地土壤有机物的施肥对

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摘要

Site specific variables and anthropogenic factors influence composition of soil organic matter (SOM). We evaluated quantity and quality of SOM under different fertilization regimes and site conditions. The study combines data based on repeated measurements obtained from six long-term field experiments, which have been established between 1955 and 1983 at ten locations, resulting in thirteen site and experiment combinations. The experimental sites cover a wide spectrum of pedological and climatic conditions of the Czech Republic. Four basic fertilization regimes were selected: unfertilized plots, mineral-only fertilized plots, plots with application of farmyard manure, and both organic and mineral fertilized plots. The study employs compositional data analysis, principal component analysis, and mixed effect linear models for statistical inference. Under combined organic and mineral fertilization, total soil organic C (SOC) increased by 1-3 g kg(-1). Evidence of possible priming effect was obtained for mineral-only fertilization. Local site conditions were the dominant factor shaping SOM properties. The positive relationship between proportion of clay in soil and decomposition index (DI) was confirmed. In the absence of fertilization, DI was eleven times higher in clay-rich than in clay-poor soil. This effect was moderated by fertilization, decreasing to a seven-fold difference under the full fertilization regime.
机译:特异性变量和人为因素影响土壤有机物的组成(SOM)。我们在不同施肥制度和现场条件下评估SOM的数量和质量。该研究结合了基于从六个长期现场实验获得的重复测量的数据,该实验已经在1955年至1983年间在十个地点建立,导致十三个网站和实验组合。实验遗址涵盖了捷克共和国的广泛的小型和气候条件。选择了四种基本施肥制度:未受精的地块,矿物施肥地块,具有野地粪便的涂层,以及有机和矿物受精地块。该研究采用组成数据分析,主成分分析和混合效应线性模型进行统计推理。在组合有机和矿物精下,总土壤有机C(SOC)增加1-3g kg(-1)。获得了可能引发效果的证据,用于矿物施肥。本地现场条件是塑造SOM属性的主要因素。确认了土壤和分解指数(DI)中粘土比例的正关系。在没有受精的情况下,富含粘土贫瘠的土壤,DI在富含粘土中的十一次。这种效果受到受精调节,在全面施肥制度下降低到七倍差异。

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